Rapid climatic changes during the Greenland stadial 1 (Younger Dryas) to early Holocene transition on the Norwegian Barents Sea coast

A pollen-based quantitative climate reconstruction from a lake-sediment core on the Norwegian Barents Sea coast provides insights about climatic change over the Greenland stadial 1 (GS-1) to early-Holocene transition. GS-1 was characterized by low July mean temperatures (c. 6.0degreesC) and dry cond...

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Bibliographic Details
Main Authors: Seppa, H, Birks, HH, Birks, HJB
Format: Article in Journal/Newspaper
Language:unknown
Published: TAYLOR & FRANCIS AS 2002
Subjects:
Online Access:http://discovery.ucl.ac.uk/155956/